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Figure 1: Preview of the published NeoNet C14 dates dataset, in red, covering the Late Mesolithic/Early Neolithic transition of the North Central-Western Mediterranean watershed

Presentation

The NeoNet app aims to contribute to the study the pioneering front of the farming live-style (i.e., Neolithic) by focusing our study on the mobile border between the Last Hunter-Gathers economy and the Early Neolithic (ca. 7,000 BC to 3,500 BC) in the Central-Western Mediterranean and European South Atlantic basins. The interactive web app facilitates the selection of absolute dates (radiocarbon dates) by providing selection tools for:

  • spatial
    • geographical region of interest (ROI)
    • custom selection shape inside the ROI
  • chronology
    • date time span between a tpq and a taq in cal BC
    • main periods (Middle Mesolithic, Late Mesolithic, Early Neolithic, …)
  • date accuracy
    • some type of material life duration (short like, long life or others)
    • threshold of the maximum accepted standard deviation (SD)

The NeoNet app has been created in the frame of the NeoNet work group from a perspective of FAIR Science and collaborative working. It is still in development. This page is a tutorial for contributing and using the app. We will see how it works, what is the format dataset and what are our objectives

NeoNet app

The app is a RShiny hosted on the Università di Pisa server. The app is divided into five (5) panels:

  1. map panel: spatial filtering with selection menus on dates
  2. calib panel: calibration of the selected dates
  3. data panel: the whole dataset
  4. biblio panel: bibliographical references
  5. infos panel: credits and link to the webpage handbook of the app

To provide a handy user interface, NeoNet app joins a main dataset with to two correspondance tables:

  • main dataset: 140_id00140_doc_elencoc14.tsv
  • bibliographical references: id00140_doc_reference.bib
  • material life duration: id00140_doc_thesaurus.tsv

So the NeoNet dataset is composed by two TSV files (dataframes with tab-separated values) and one BIB file (BibTex file, see: NeoNet dataset v.1


1. map panel

The panel map is a geographical window provided by the Leaflet package. This panel is used for selection of radiocarbon dates by location, by chronology, by quality of dates. Once selected, dates can be calibrated

The different menus of the map panel

Figure 2: The different menus of the map panel

The current functions are:

  • Fig. 2, red box, top-left radio button group C14 on map: allows to cluster dates by spatial proximities (Marker Clusters)

  • Fig. 2, pink box, top-right layer button: allows to change the basemap. By default, the basemap is OSM, an OpenStreetMap general basemap, but it can be switch to Topo, an ESRI topographical basemap

  • Fig. 2, green box, inline text: reactive count of selected dates and sites. The bottom table is a reactive DT package datatable listing all the dates within the map extent (ROI) and the optional selection menus (tpq/taq, material life duration, maximum SD, periods, selection shapes)

select by location

By default only the data within the window extent (ROI) will be selected. But selection shapes can be drawn inside this ROI to have a spatial intersection:

Fig. 2, black box, top-left draw toolbar: selection shapes, polygons and rectanges, can freeze the date selection inside a given ROI. They can be removed with the trash button. All the dates inside the ROI and selected with the others filters will be visible on the map, but only those inside the selections shapes will be calibrated

selection inside a shape, here a single polygon. Before shape selection: 190 sites and 895 dates. After shape selection: 13 sites and 68 dates

retrieve coordinates from the map

As said, the default basemap of the app is OSM. It offers a well documented basemap where archaeological sites are sometimes already located, like the Ligurian site of Grotta della Pollera. Clicking on the map show the lat/long coordinates of the current point (under the tpq/tap slider). These coordinates can then be copied and used to modify the NeoNet dataset

get coordinates by clicking on the map

select by chronology

  • Fig. 2, brown box, top-right checkboxes: allow to select dating by periods. The orange box, bottom-left legend, is reactive and update depending on selected periods

  • Fig. 2, blue box, bottom-left slider: allows to subset a range of accepted dates between a tpq and a taq (in cal BC)

select by dates quality

  • Fig. 2, purple box, bottom-right checkboxes and slider: a group of menus for selection on the material life duration and max accepted SD:
  • relatively to the duration of their material (short to long-life material)
  • below a maximum accepted threshold for the standard deviations (SD) for the dates

calibrate one or various dates

The dates displayed in the table of the map panel will be calibrate when one of them has been clicked.

click on a date to calibrate a selected group of dates

2. calib panel

The panel calib is used for analysis. Calibration of selected dates are done on-the-fly with the R package rcarbon. If the dates are numerous (e.g., > 100) the computing time could take times, be patient.

calibration of selected radiocarbon dates

This date which have been clicked on the map panel will be shown bolded on the output figure

C14 group by filter

The c14 group by filter (Fig. 3, red box) allows to plot dates and to sum their probability densities depending on different levels of grouping:

  • by datation (by LabCode). Each radiocarbon date is plot separately (by default)

  • by site and layer (= SiteName and PhaseCode). Dates from the same site, having the same archaeological unit (layer, structure, etc.), are summed. See the PhaseCode field.

  • by site and period (= SiteName and Period). Dates from the same site, having the same period are summed

  • by period (= Period). Dates having the same period are summed

  • all C14. All dates are summed

The different menus of the calib panel

Figure 3: The different menus of the calib panel

plot area output

The plot area (Fig. 3, orange box) shows dynamically the SPD of the cabibrated dates seriated on their weighted means. The top-right button Download (Fig. 3, green box) allows to export the last plot in a PNG image

3. data panel

The complete dataset from the GitHub 140_140_id00140_doc_elencoc14.tsv file (ie, NeoNet dataset v.1). Today, the dataset counts 2506 dates:

Table 1: Dates sample
SiteName Country Period PhaseCode LabCode C14Age C14SD Material MaterialSpecies tpq taq Longitude Latitude bib bib_url
Mala Triglavca Slovenia LMEN Grid 7, Layer 2.90-3.05 OxA-15139 6451 36 animal bone Cervus sp. -5479 -5332 13.956800 45.67440 Mlekuz et al. 2008 https://doi.org/10.4312/dp.35.18
Grotta della Serratura Italy MN Layer 1-3 UtC-747 6030 130 wood charcoal n/d -5301 -4614 15.386400 39.99720 Colonese et al. 2010 https://doi.org/10.1016/j.gloplacha.2009.05.006
Jacmica Cave Croatia MN n/a OxA-18181 6191 31 wood charcoal Fraxinus sp. -5287 -5040 13.945246 45.44290 Forenbaher & Miracle 2014 Forenbaher14
Plansallosa Spain MN Layer II OxA-2592 5890 80 wood charcoal n/d -4982 -4546 2.632176 42.23421 Tabernero et al. 1999 Tabernero99
Grotta dell’Edera Italy MN Layer 2 GrN-26797 5080 40 wood charcoal mainly Corylnus, also Quercus & Fraxinus sp. -3969 -3781 13.696400 45.75690 Bonizzoni et al. 2009 https://doi.org/10.1111/j.1475-4754.2008.00412.x
Scamuso Italy EN Trench A III, tg. 15 Gif-6338 5290 90 wood charcoal n/d -4331 -3961 17.039166 41.07750 Rosini et al. 2005 Rosini05

At first, these data were recorded in an Excel-like spreadsheet in order to facilitate their editing (filter, sorting, filling). As data came from various publications, a homogenization the different values (material, cultures, bibliographical references, etc.) has been done. The dataset mandatory fields are:

The recommended fields are:

  • Culture: a specification of the field Period

mandatory fields

Here we explain more precisely some of the mandatory fields

SiteName

The most accepted version of the site name. For example: Cova de l'Or offers a better designation than L'Or or Or.

Longitude and Latitude

In decimal degrees and a minimal precision of four (4) decimal digits (ex: 1.0453, 43.9211). Since the NeoNet modeling is supra-regional, the app does not need to record dates with high accuracy geographical coordinates. At the minimum, this accuracy can be a location inside the departmental/county boundaries (how to retrieve better coordinates from the map)

Period

The period abbreviation. The main common periods considered here are: LM (Late Mesolithic), UM (Undefined Mesolithic), LMEN (Late Mesolithic/Early Neolithic), EN (Early Neolithic), MN (Middle Neolithic), LN (Late Neolithic), UN (Undefined Neolithic)

periods names colors
EM Early Mesolithic #0000CF
MM Middle Mesolithic #1D1DFF
LM Late Mesolithic #3737FF
LMEN Late Mesolithic/Early Neolithic #6A6AFF
UM Undefined Mesolithic #8484FF
EN Early Neolithic #FF1B1B
EMN Early/Middle Neolithic #FF541B
MN Middle Neolithic #FF8D1B
LN Late Neolithic #FFC04D
UN Undefined Neolithic #E7E700

By default a different hexadecimal color is attributed to each period

PhaseCode

The PhaseCode field provides information about the archaeological context of a given date within a site. In most cases, it corresponds to an archaeological layer or structure. It is useful for layer/structure C14 grouping.

PhaseCode
UE3002
Layer 20, Hearth 7
Layer 9
A, near vessel 2169
CA1
GC1-PC1

At the site scale, these field values need to be homogeneized (for example: C.5 or layer 5 -> C5). The n/a value (i.e., not available) is reserved to dates without intra-site contextual information

LabCode

LabCode (i.e., laboratory code) should be unique. Their conventional syntax is ‘AbrevLab-number’, respecting the case letters (upper case and lower case). For example:

LabCode
Ly-4415(SacA-8117)
MC-781
Poz-36646
R-313
Ly-7347(SacA-20965)
Ly-12107(SacA-41853)

See also the list of laboratories. Exceptionally, if a date has no LabCode – e.g., ‘Sep-H3 mix’ from Fontbregoua, 6082 +/- 35 BP – the convention is to use the PhaseCode (e.g., ‘Sep-H3 mix’) with an underscore as a prefix (e.g., ‘_Sep-H3 mix’) to get an unique key.

C14Age and C14SD

Conventional radiocarbon uncalibrated date (C14Age) and standard deviation error (C14SD). These two fields are used to calibrated the radiocarbon dates and calculate the tpq (terminus post quem) and taq (terminus ante quem).

C14Age C14SD
5895 55
6669 34
5220 100
7010 40
6793 40
7425 55
Material

Material life duration are read from the GitHub 140_id00140_doc_thesaurus.tsv file (ie, NeoNet dataset v.1. The two fields show the material type (column 1) and the material life duration (column 2), for example:

material.type life.duration
Collagene C capreolus short.life
Llavor short.life
Monocotil
Semillas carbonizadas short.life
WC long.life
Hordeum v short.life

Among these values, the published NeoNet dataset uses uniquely these ones:

Material
animal bone
human and animal bone
human bone
n/a
n/d
organic
plant seed
shell
wood charcoal
wood charcoal or plant seeds

The join between the main dataset and the material life thesaurus gives:

material.type life.duration
animal bone short.life
human bone short.life
n/a
n/d
organic short.life
plant seed short.life
shell long.life
wood charcoal long.life
MaterialSpecies
bib and bib_url

Every radiocarbon date should be referenced with (i) a short plain text bibliographical reference (bib field) and (ii) a DOI or, when missing, a BibTex key (bib_url field). We favor the earliest mention of the radiocarbon date.

bib

The plain text that will be plot for each radiocarbon date under the bibliographical reference section. Basically the name of the author(s) and the publication year, for example Guilaine et al. 1993, Binder 2018 or Manen et Sabatier 2013. The values of this field can be the same for two different publications (e.g. Delibrias et al. 1982 refers to two different publications the same year)

bib_url

Either a DOI or a unique BibTeX key. We favor the DOI as a unique bibliographical reference. The values of this field should be unique for a single publication (e.g. the BibTeX keys Delibrias82 and Delibrias82a). For example:

bib bib_url
Gonzalez et al. 2011 Gonzalez11
Natali & Forgia 2018 https://doi.org/10.1016/j.quaint.2017.07.004
Gonzalez-Samperiz et al. 2008 https://doi.org/10.1016/j.yqres.2008.10.006
Binder et al. 2018 https://doi.org/10.4312/dp.44.4
Manen & Sabatier 2003 https://doi.org/10.3406/bspf.2003.12868
Gonzalez-Samperiz et al. 2008 https://doi.org/10.1016/j.yqres.2008.10.006
  • the DOI exists: Add the DOI value to the field. The DOI value starts with “10

  • the DOI doesn’t exists: The complete bibliographical reference has to be included into the BIB document (eg., id00140_doc_reference.bib). In the BIB file, the bibliographical reference keyis the name of the first author and the two last digits of the year (eg., Guilaine93):

@book{Guilaine93,
  title={Dourgne: derniers chasseurs-collecteurs et premiers {\'e}leveurs de la Haute-Vall{\'e}e de l'Aude},
  author={Guilaine, Jean and Barbaza, Michel},
  year={1993},
  publisher={Centre d'anthropologie des soci{\'e}t{\'e}s rurales; Arch{\'e}ologie en Terre d'Aude}
}

The same key of this reference is added to the bib_url field. For example, the key value Guilaine93 to map the main dataset to the BIB file.

bib bib_url
Guilaine et al. 1993 Guilaine93

4. biblio panel

Bibliographical references are recorded in id00140_doc_reference.bib file. If only exist a BibTeX key, and no DOI, this file results of the join between the bib_url field of the C14 spreadsheet and the BIB file.

@Article{Binder18,
  title = {Modelling the earliest north-western dispersal of Mediterranean Impressed Wares: new dates and Bayesian chronological model},
  author = {Didier Binder and Philippe Lanos and Lucia Angeli and Louise Gomart and Jean Guilaine and Claire Manen and Roberto Maggi and Italo M Muntoni and Chiara Panelli and Giovanna Radi and others},
  journal = {Documenta praehistorica},
  volume = {44},
  pages = {54-77},
  year = {2018},
  publisher = {University of Ljubljana Department of Archaeology},
}

@InProceedings{Briois09,
  title = {L'abri de Buholoup: de l'{\'E}pipal{\'e}olithique au N{\'e}olithique ancien dans le piedmont central des Pyr{\'e}n{\'e}es},
  author = {François Briois and Jean Vaquer},
  booktitle = {De M{\'e}diterran{\'e}e et d'ailleurs...: m{\'e}langes offerts {\`a} Jean Guilaine},
  pages = {141-150},
  year = {2009},
}

In the app, this BibTex file is rendered in HTML with an APA citation format (field long.ref) with the read.bib() and the markdown() functions (among others).

5. infos panel

Infos & credits

Developments

The NeoNet dataset will be extended to the European South Atlantic river basin (ie. Portugal, western Spain, and southwest France)

Figure 4: Preview of the future NeoNet dataset, in blue, covering the Middle and Southern European Atlantic watershed

Milestones

NeoNet workgroup, and NeoNet app, aim to facilitate contributions in a perspective of FAIR Science. In practical terms, we have planned to:

  • host the app and dataset on an institutional web server
  • publish the dataset in an Open Data repository to get a DOI
  • submit the dataset in a data paper (JOAD)
  • open the app to new contributions
  • create a connector to the dataset with the c14bazAAR getter function
  • publish the app source code in an Open digital humanities paper (ex: JOSS)

Credits

Currently, the NeoNet database and app received the contributions of the NeoNet workgroup collaborators:

The NeoNet Mediteranean dataset has been published in the Journal of Open Archaeology Data under this BibTex reference:

@article{Huet22,
author = {Huet, Thomas and Cubas, Miriam and Gibaja, Juan .F. and Oms, F. Xavier and Mazzucco, Niccolo},
title = {NeoNet Dataset. Radiocarbon Dates for the Late Mesolithic/Early Neolithic Transition in the North Central-Western Mediterranean Basin},
journal = {Journal of Open Archaeology Data},
year = {2022},
volume = {10},
number = {3},
pages = {1-8},
doi={10.5334/joad.87},
}

The development version of the app is on GitHub: zoometh/neonet where you can check the contribution rules and the relevant license.

Acknowledgement

We are especially thankful to Federico Bianchi of the University of Pisa for the technical support